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Question 1
ప్రశ్న 1
Why must seepage be controlled in an earth dam even though some seepage through soil is normally unavoidable?
Explanation:
Earth and rockfill dams normally experience some seepage through the embankment, foundation, or abutments. The design objective is therefore to control seepage rather than assume that absolutely no water will pass through the system. Excess pore-water pressure can reduce effective stress and adversely affect slope stability. Concentrated or high-gradient seepage can also detach and transport soil particles, leading to internal erosion or piping. Therefore Option B is correct.
వివరణ:
Question 2
ప్రశ్న 2
In an earth-dam cross-section under steady seepage, what is the phreatic surface?
Explanation:
The phreatic surface is the upper seepage surface in the embankment or foundation under the condition being considered. Gauge pore-water pressure on this surface is zero because the water pressure equals atmospheric pressure. In a two-dimensional dam cross-section, this surface is commonly shown as the phreatic line. Below it, pore-water pressures are generally positive under ordinary saturated seepage conditions. Therefore Option C is correct.
వివరణ:
Question 3
ప్రశ్న 3
Which statement about pore-water pressure below the phreatic surface is generally correct for steady seepage in an earth dam?
Explanation:
The phreatic surface marks zero gauge pore-water pressure, not zero pressure throughout the saturated zone. At points below it, positive pore-water pressure commonly develops. Effective stress is the difference between total stress and pore-water pressure. An increase in pore pressure at unchanged total stress therefore reduces effective stress and can reduce available shear strength. Hence Option A is correct.
వివరణ:
Question 4
ప్రశ్న 4
What is the principal concern if the phreatic surface in an earth dam rises unusually high and approaches or intersects an unprotected downstream slope?
Explanation:
A high phreatic surface means that a greater part of the downstream embankment is subjected to seepage and pore pressure. This reduces effective stress compared with a well-drained condition. Seepage emerging directly on an unprotected downstream slope can also cause local erosion or softening. Shallow sloughing or a deeper slope-stability problem may then develop depending on the soils and geometry. Therefore Option D is correct.
వివరణ:
Question 5
ప్రశ్న 5
Why is a chimney filter or drain connected to a horizontal drainage blanket commonly placed downstream of the impervious core?
Explanation:
A downstream chimney filter or drain intercepts seepage passing through defects in or around the low-permeability zone. Proper filter gradation helps prevent protected soil particles from being carried into the drainage material. The connected horizontal blanket provides a low-resistance path toward a safe downstream outlet. This arrangement can lower pore pressures and keep the phreatic surface away from much of the downstream slope. Therefore Option B is correct.
వివరణ:
Question 6
ప్రశ్న 6
Which description best represents backward-erosion piping in the foundation or embankment of an earth dam?
Explanation:
Backward-erosion piping begins when seepage forces detach soil particles near an unprotected exit or other vulnerable location. Continued particle removal causes the erosion feature to progress in the upstream direction against the seepage flow. If progression is not arrested, a continuous high-flow path can develop through the foundation or embankment. This mechanism is one form of internal erosion and should not be confused with ordinary clear seepage through a stable filter. Therefore Option C is correct.
వివరణ:
Question 7
ప్రశ్న 7
A transverse crack develops through the impervious core because of differential settlement, and reservoir water begins flowing through the crack and eroding its walls. Which failure mechanism is most directly represented?
Explanation:
A crack can create a preferential path through which water flows at a much greater local velocity than through intact compacted soil. Flow along the crack can detach material from the crack walls and enlarge the seepage path. This process is commonly described as concentrated-leak internal erosion. A properly designed downstream filter is an important defensive feature because it can retain eroded core material and limit progression. Hence Option A is correct.
వివరణ:
Question 8
ప్రశ్న 8
During inspection of an earth dam, which observation most strongly suggests that internal erosion may be actively transporting soil?
Explanation:
Seepage quantity, location, and clarity are important indicators of embankment performance. New or increasing turbid seepage can indicate that soil particles are being detached and transported by flowing water. Such a condition may represent an active internal-erosion process and requires prompt engineering evaluation. Clear seepage can also warrant investigation if its rate or location changes significantly, but visible transported soil is a particularly serious warning sign. Therefore Option D is correct.
వివరణ:
Question 9
ప్రశ్న 9
What combination of properties is required of a granular filter protecting a fine-grained earth-dam core?
Explanation:
A protective filter has two requirements that must be satisfied together. Its void sizes must be small enough to prevent unacceptable movement of particles from the protected soil. At the same time, it must be permeable enough to transmit seepage without developing excessive hydraulic gradients or pore pressures. A filter is therefore neither simply an impervious barrier nor an unrestricted coarse drain. Hence Option B is correct.
వివరణ:
Question 10
ప్రశ్న 10
Which statement correctly distinguishes the functions of a filter and a drain in an earth dam?
Explanation:
Filters and drains often use similar granular materials, but their functional emphasis is not identical. A filter is proportioned to prevent unacceptable migration of the soil it protects while allowing seepage to cross the interface. A drain must additionally have sufficient permeability and geometry to collect and convey the expected seepage flow. Many embankment systems therefore use compatible filter and drainage zones together. Therefore Option C is correct.
వివరణ:
Question 11
ప్రశ్న 11
What is the principal benefit of a properly designed toe drain at the downstream toe of an earth dam?
Explanation:
A toe drain receives seepage from internal filters, drainage blankets, or the foundation. It then conveys this water to a safe and observable outlet. By providing a controlled exit, the drain helps reduce uncontrolled seepage emergence and saturation near the downstream toe. The drain itself must be protected by suitable filters so that soil is not washed into it. Therefore Option A is correct.
వివరణ:
Question 12
ప్రశ్న 12
What is the main seepage-control effect of a cutoff trench or cutoff wall extending into a pervious foundation beneath an earth dam?
Explanation:
A pervious foundation can transmit water beneath the embankment even when the dam core itself has low permeability. A cutoff introduces a low-permeability barrier into this seepage path. This increases the resistance to underseepage and can reduce seepage quantity and adverse downstream gradients. A partial cutoff does not necessarily eliminate seepage, so drainage or other measures may still be required. Therefore Option D is correct.
వివరణ:
Question 13
ప్రశ్న 13
In an idealized seepage calculation, hydraulic conductivity is 2 × 10^-6 m/s, hydraulic gradient is 0.50, and the flow area normal to seepage is 30 m² per metre length of dam. Using Darcy's law, what is the seepage discharge per metre length?
Explanation:
Darcy's law gives discharge as q = k i A for the stated idealized condition. Substitution gives q = 2 × 10^-6 × 0.50 × 30 = 3 × 10^-5 m³/s. Multiplying by 1000 converts this value to 0.030 L/s. The result applies only to the stated hydraulic conductivity, gradient, and flow area and should not be interpreted as a complete dam seepage analysis. Therefore Option B is correct.
వివరణ:
Question 14
ప్రశ్న 14
A seepage path has a total head loss of 12 m over an idealized flow length of 60 m. What is the average hydraulic gradient along that path?
Explanation:
Hydraulic gradient is the head loss divided by the corresponding seepage length for this simplified calculation. The head loss is 12 m and the length is 60 m. Thus i = 12/60 = 0.20. Actual seepage gradients in a dam vary spatially, so a single average value does not describe local exit conditions. Therefore Option C is correct.
వివరణ:
Question 15
ప్రశ్న 15
For an ideal saturated cohesionless soil, the critical upward hydraulic gradient may be estimated as i_cr = (G_s - 1)/(1 + e). If G_s = 2.65 and void ratio e = 0.65, what is i_cr?
Explanation:
The stated expression gives the critical hydraulic gradient for the ideal upward-seepage condition. Substitution gives i_cr = (2.65 - 1)/(1 + 0.65) = 1.65/1.65 = 1.00. As upward gradient approaches this value, seepage force can reduce effective stress toward zero and promote boiling or heave. This simplified quick-condition criterion is related to seepage instability but is not a complete model of every internal-erosion or piping mechanism in a dam. Therefore Option A is correct.
వివరణ:
Question 16
ప్రశ్న 16
At a point in a saturated earth-dam slope, the total normal stress is 180 kPa and pore-water pressure is 70 kPa. What is the effective normal stress at that point?
Explanation:
Effective stress is obtained by subtracting pore-water pressure from total stress. The total normal stress is 180 kPa and the pore pressure is 70 kPa. Hence the effective normal stress is 180 - 70 = 110 kPa. If pore pressure increased while total stress remained unchanged, the effective stress would decrease and the available frictional shear strength would generally be reduced. Therefore Option D is correct.
వివరణ:
Question 17
ప్రశ్న 17
Under prolonged full-reservoir conditions after steady seepage has developed, which slope of a conventional earth dam commonly requires particular seepage-related stability attention?
Explanation:
With the reservoir maintained high for a sufficiently long period, seepage conditions can approach steady state. Pore-water pressures then develop through the embankment and foundation according to the seepage field. The downstream slope can contain significant pore pressures, especially if drainage is inadequate or the phreatic surface is high. These pore pressures reduce effective stress and can lower the factor of safety of the downstream slope. Therefore Option B is correct.
వివరణ:
Question 18
ప్రశ్న 18
Why is rapid drawdown of the reservoir commonly a critical loading condition for the upstream slope of an earth dam?
Explanation:
Before drawdown, the upstream portion of the embankment may contain substantial pore-water pressure. Rapid reservoir lowering removes part of the external water pressure that had been supporting the upstream face. In low-permeability material, internal pore pressures cannot dissipate at the same rate as the reservoir falls. The resulting reduction in effective stress can make the upstream slope significantly less stable. Therefore Option C is correct.
వివరణ:
Question 19
ప్రశ్న 19
For a simplified slope-stability calculation, the available resisting shear force along an assumed slip surface is 1950 kN per metre length and the mobilized driving shear force is 1300 kN per metre length. What is the corresponding factor of safety?
Explanation:
For the stated simplified force-ratio definition, the factor of safety is resisting shear divided by driving shear. The resisting force is 1950 kN/m and the driving force is 1300 kN/m. Thus the factor of safety is 1950/1300 = 1.50. A real earth-dam stability analysis requires appropriate pore pressures, shear-strength parameters, geometry, and loading conditions in addition to this elementary ratio. Therefore Option A is correct.
వివరణ:
Question 20
ప్రశ్న 20
What is meant by sloughing of the downstream slope of an earth dam in a seepage-distress context?
Explanation:
Sloughing commonly refers to localized loss of stability in near-surface material rather than a large deep-seated slide. On an earth dam, it may occur where seepage saturates and softens part of the downstream face. The accompanying rise in pore pressure lowers effective stress and can reduce available shear resistance. Drainage and control of the phreatic surface are therefore important measures against seepage-related sloughing. Hence Option D is correct.
వివరణ:
Question 21
ప్రశ్న 21
Why is uncontrolled overtopping especially dangerous for a conventional earth dam?
Explanation:
Conventional earth embankments are not intended to carry uncontrolled spillway flow over their crests. Water flowing down the downstream face can remove protective cover and erode compacted fill. Once a channel develops, increasing concentration of flow can accelerate erosion and deepen the breach. Adequate spillway capacity, freeboard, crest maintenance, and settlement allowance are therefore fundamental overtopping defenses. Hence Option B is correct.
వివరణ:
Question 22
ప్రశ్న 22
How can differential settlement increase the risk of internal erosion in an earth dam?
Explanation:
Different parts of an embankment or its foundation may settle by different amounts. The resulting tensile deformation can crack an impervious core or open interfaces near steep abutments and structures. A crack may form a preferential seepage path with much higher local flow than intact soil would carry. If downstream filters do not safely retain eroded particles, concentrated-leak internal erosion can progress. Therefore Option C is correct.
వివరణ:
Question 23
ప్రశ్న 23
Why is a transverse crack through an earth-dam core generally of greater internal-erosion concern than a longitudinal crack that does not cross the core?
Explanation:
A transverse crack can cut across the low-permeability barrier in the general upstream-to-downstream seepage direction. It may therefore create a concentrated path connecting reservoir water to downstream zones. Flow through such a defect can initiate erosion of the crack walls if the core material is erodible. Longitudinal cracks may still be important for slope stability, especially if they fill with water, but they do not necessarily create the same direct cross-core seepage path. Hence Option A is correct.
వివరణ:
Question 24
ప్రశ్న 24
Which monitoring pattern should cause particular concern for seepage and stability performance of an earth dam?
Explanation:
Earth-dam distress is often detected through changes rather than through a single isolated measurement. Rising piezometric levels can indicate increasing pore pressures or deterioration of drainage performance. New wet areas, increasing seepage, or turbid discharge can signal a developing seepage path or internal erosion. Sinkholes, cracking, and unusual settlement can indicate material loss or differential deformation and must be interpreted together with reservoir conditions. Therefore Option D is correct.
వివరణ:
Question 25
ప్రశ్న 25
An earth dam develops a new wet area on its downstream slope, drain discharge is increasing and becoming muddy, and nearby piezometers show rising pore-water levels. What is the most appropriate engineering interpretation?
Explanation:
The three observations together are more significant than any one of them in isolation. Rising pore pressures can reduce slope stability, while increasing seepage indicates a change in the hydraulic response of the dam. Turbidity suggests that soil particles may be moving, which raises concern for active internal erosion. Simply sealing a downstream seepage outlet can increase pore pressures or redirect flow unless a properly engineered measure is used. Therefore Option B is correct.
వివరణ:
Answer Key సమాధానాల పట్టిక
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Question 1 ప్రశ్న 1Answer: B. Because uncontrolled seepage can raise pore pressures, destabilize the downstream slope, and initiate internal erosion or piping సమాధానం: B.
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Question 2 ప్రశ్న 2Answer: C. The seepage surface along which pore-water pressure is atmospheric, represented as a line in a two-dimensional cross-section సమాధానం: C.
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Question 3 ప్రశ్న 3Answer: A. Positive pore-water pressure may exist below the phreatic surface and reduces effective stress relative to the same total stress with lower pore pressure సమాధానం: A.
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Question 4 ప్రశ్న 4Answer: D. It can saturate the downstream zone, increase pore pressures, and promote seepage emergence, sloughing, or instability సమాధానం: D.
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Question 5 ప్రశ్న 5Answer: B. To intercept seepage, protect against migration of fine particles, and convey water safely toward the downstream toe సమాధానం: B.
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Question 6 ప్రశ్న 6Answer: C. Progressive removal of soil beginning near a seepage exit and advancing backward toward the water source, potentially forming a continuous pipe సమాధానం: C.
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Question 7 ప్రశ్న 7Answer: A. Concentrated-leak internal erosion సమాధానం: A.
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Question 8 ప్రశ్న 8Answer: D. A new or increasing muddy seepage discharge carrying visible soil particles సమాధానం: D.
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Question 9 ప్రశ్న 9Answer: B. It should be fine enough to retain the protected soil yet sufficiently permeable to pass seepage without excessive pressure buildup సమాధానం: B.
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Question 10 ప్రశ్న 10Answer: C. A filter primarily protects soil against particle migration while allowing water passage, whereas a drain must also provide adequate capacity to collect and convey seepage సమాధానం: C.
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Question 11 ప్రశ్న 11Answer: A. It provides a controlled outlet for intercepted seepage and helps prevent uncontrolled saturation and seepage emergence on the downstream slope సమాధానం: A.
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Question 12 ప్రశ్న 12Answer: D. It reduces underseepage by increasing flow resistance and, depending on its depth and continuity, can reduce downstream gradients and uplift సమాధానం: D.
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Question 13 ప్రశ్న 13Answer: B. 0.030 L/s సమాధానం: B.
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Question 14 ప్రశ్న 14Answer: C. 0.20 సమాధానం: C.
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Question 15 ప్రశ్న 15Answer: A. 1.00 సమాధానం: A.
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Question 16 ప్రశ్న 16Answer: D. 110 kPa సమాధానం: D.
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Question 17 ప్రశ్న 17Answer: B. The downstream slope, because seepage pore pressures and the phreatic surface can reduce effective stress there సమాధానం: B.
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Question 18 ప్రశ్న 18Answer: C. Because external reservoir support can fall rapidly while pore-water pressures within low-permeability upstream fill dissipate much more slowly సమాధానం: C.
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Question 19 ప్రశ్న 19Answer: A. 1.50 సమాధానం: A.
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Question 20 ప్రశ్న 20Answer: D. Local or shallow sliding and softening of downstream slope material, often associated with saturation or seepage emerging from the embankment సమాధానం: D.
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Question 21 ప్రశ్న 21Answer: B. Because flow over the crest and downstream face can rapidly erode earth materials, enlarge a breach, and lead to progressive failure సమాధానం: B.
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Question 22 ప్రశ్న 22Answer: C. It can produce cracks or poorly compressed interfaces that become preferential seepage paths and allow concentrated-leak erosion to initiate సమాధానం: C.
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Question 23 ప్రశ్న 23Answer: A. A transverse crack can provide a direct preferential seepage path from the reservoir side toward the downstream side సమాధానం: A.
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Question 24 ప్రశ్న 24Answer: D. Rising piezometric levels, increasing or newly located seepage, turbidity, wet spots, sinkholes, cracking, or unexplained settlement సమాధానం: D.
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Question 25 ప్రశ్న 25Answer: B. The combination is potentially indicative of deteriorating seepage control or internal erosion and requires prompt investigation while maintaining or restoring safe filtered drainage rather than simply blocking the seepage exit సమాధానం: B.
